CYCLONE NISARGA IN MUMBAI
Cyclone Nisarga’s landfall at
Murud in Raigad district of Maharashtra on June 3.
Nisarga was categorised as a
severe cyclone
Cyclone: It is a large scale air mass that rotates around a strong centre of low atmospheric pressure
The
largest low-pressure systems are polar vortices and extratropical
cyclones of the
largest scale (the synoptic
scale).
Warm-core
cyclones such as tropical
cyclones and subtropical
cyclones also lie
within the synoptic scale.
Cyclogenesis
is the development or strengthening of cyclonic circulation in the atmosphere.
Cyclolysis
is the opposite of cyclogenesis, and is the high-pressure system equivalent,
which deals with the formation of high-pressure
areas—Anticyclogenesis.
Cyclones
can transition between extratropical, subtropical, and tropical phases.
Mesocyclones form as warm core cyclones over land, and can lead to tornado formation.
Because
of the Coriolis
effect, the wind flow
is counterclockwise in the Northern Hemisphere and clockwise in the Southern
Hemisphere.
3 main
types of surface-based cyclones: Extratropical
cyclones, Subtropical
cyclones and Tropical cyclones
Extratropical cyclone: Cyclones outside the tropics, in the middle
latitudes.
Extratropical
cyclones are almost classified as baroclinic since they form along zones of
temperature and dewpoint gradient within the westerlies,
Subtropical cyclone: Some
characteristics of a tropical cyclone and some characteristics of an extratropical
cyclone.
Broad
wind patterns with maximum sustained winds located farther from the center than
typical tropical cyclones, and exist in areas of weak to moderate temperature
gradient
Tropical: A tropical cyclone is a storm system characterized by a low-pressure center and numerous thunderstorms that produce strong winds and flooding rain.
Depending
on their location and strength, tropical cyclones have different names, such as
hurricane, typhoon, tropical storm, cyclonic storm,
tropical depression, or simply as a cyclone.
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